Na 50 Nachlass Arthur Schopenhauer - 'Schopenhauer-Archiv', 921 - Plan einer Biographie über Arthur Schopenhauer

u.a. Erbe;

Ms.Ff.F.Stoltze 3. 153 - Brief von Otto Kanngießer an Friedrich Stoltze

Kondolation zum Tode Marie Stoltzes

Na 1 Nachlass Max Horkheimer, 688 - "Fortune Polls on Antisemitism" (p. IX 153.1-18)

"Fortune Polls on Antisemitism" (1947) (veröffentlicht unter dem Titel "Fortune Survey Analyzed by AJC Consultant to Appraise Results", in: News Letter, American Jewish Committee, Dezember 1947, S. 4):; 1. Max Horkheimer: Über Fortune Polls, a) Typoskript, 3 Blatt, b) Typoskript, 3 Blatt, c) Typoskript mit eigenhändigen Korrekturen, 3 Blatt, d) Typoskript, 3 Blatt; 2. Max Horkheimer: Über Fortune Polls und die Gefahren eines neuen Antisemitismus (Vortragsskript?), Typoskript und Manuskript, 4 Blatt; 3. Theodor W. Adorno (?): "Some Results of Adult Project". Typoskript mit eigenhändigen Korrekturen, 2 Blatt; 4. "Education Counteracts Prejudice" Auszug aus "Antisemitism among American Labor". Typoskript, 1 Blatt; 5. "Discord versus Harmony", Excerpt from: The Annals of the American Academy of Political and Social Science, March 1946, Typoskript, 1 Blatt; 6. Theodor W. Adorno: "Memorandum, Subject: Poll Controversy", 24.4.1948; 7. Leo Löwenthal: "Memorandum on Fortune Poll" und "Supplementary Memorandum on Fortune Poll", 8.10.1947. Typoskripte mit eigenhändigen Ergänzungen, 4 Blatt; 8. "Massing's Comment" (8.10.1947). Typoskript, 2 Blatt; 9. "Excerpts from Fortune Magazine 'The Fortune Survey': Racial and Religious Intolerance". Typoskript, 3 Blatt, a) "Summary of 'Fortune Survey' on Antisemitism in U.S. (Fortune, April, 1939)", Typoskript, 2 Blatt; 10. Leo Löwenthal: 1 Brief mit Unterschrift an Max Horkheimer, New York, 4.10.1947, 1 Blatt; 11. Exzerpt der Umfrage-Materialien der Opinion Research Corporation, Typoskripte, 61 Blatt; 12. Zahlenmaterial zu den Umfragen, 16 Blatt; Office of War Information, Bureau of Intelligence: Berichte über Antisemitismus: 13. "Attitudes toward Jews in the United States", 27.10.1942, a) als Typoskript vervielfältigt, 22 Blatt, b) Typoskript, 35 Blatt; 14. "Political Anti-Semitism: A Study of Indoctrination" (27.10.1942), a) als Typoskript vervielfältigt, 18 Blatt, b) Typoskript, 26 Blatt; 15. "Anti-Semitism - a Symptom of Disaffection" (8.10.1942), a) als Typoskript vervielfältigt, 8 Blatt, b) Typoskript, 12 Blatt; 16. Samuel H. Flowerman und Marie Jahoda: "Polls on Anti-Semitism. How much do they tell us?", Sonderdruck, 4 Blatt; 17. Fragebogen, Drucksachen, 4 Blatt; 18. Zeitungausschnitte aus: The Fortune Survey, 9 Blatt;

Ms. lat. oct. 153 - Theologische Sammelhandschrift

Vorbesitzer: Bernhard Diell;

Element concentrations of plagioclase and clinopyroxene in poikilitic olivine gabbros from ODP Hole 153-923A (Table 4)

Ocean Drilling Program Hole 923A, located on the western flank of the Mid-Atlantic Ridge south of the Kane Fracture Zone, recovered primitive gabbros that have mineral trace element compositions inconsistent with growth from a single parental melt. Plagioclase crystals commonly show embayed anorthitic cores overgrown by more albitic rims. Ion probe analyses of plagioclase cores and rims show consistent differences in trace element ratios, indicating variation in the trace element characteristics of their respective parental melts. This requires the existence of at least two distinct melt compositions within the crust during the generation of these gabbros. Melt compositions calculated to be parental to plagioclase cores are depleted in light rare earth elements, but enriched in yttrium, compared to basalts from this region of the Mid-Atlantic Ridge, which are normal mid-ocean ridge basalt (N-MORB). Clinopyroxene trace element compositions are similar to those predicted to be in equilibrium with N-MORB. However, primitive clinopyroxene crystals are much more magnesian than those produced in one-atmosphere experiments on N-MORB, suggesting that the major element composition of the melt was unlike N-MORB. These data require that the diverse array of melt compositions generated within the mantle beneath mid-ocean ridges are not always fully homogenised during melt extraction from the mantle and that the final stage of mixing can occur efficiently within crustal magma chambers. This has implications for the process of melt extraction from the mantle and the liquid line of descent of MORB

Granulometry of two sediment cores from Maxwell Bay, South Shetland Islands, West Antarctica

The climate evolution of the South Shetland Islands during the last c. 2000 years is inferred from the multiproxy analyses of a long (928 cm) sediment core retrieved from Maxwell Bay off King George Island. The vertical sediment flux at the core location is controlled by summer melting processes that cause sediment-laden meltwater plumes to form. These leave a characteristic signature in the sediments of NE Maxwell Bay. We use this signature to distinguish summer and winter-dominated periods. During the Medieval Warm Period, sediments are generally finer which indicates summer-type conditions. In contrast, during the Little Ice Age (LIA) sediments are generally coarser and are indicative of winter-dominated conditions. Comparison with Northern and Southern Hemisphere, Antarctic, and global temperature reconstructions reveals that the mean grain-size curve from Maxwell Bay closely resembles the curve of the global temperature reconstruction. We show that the medieval warming occurred earlier in the Southern than in the Northern Hemisphere, which might indicate that the warming was driven by processes occurring in the south. The beginning of the LIA appears to be almost synchronous in both hemispheres. The warming after the LIA closely resembles the Northern Hemisphere record which might indicate this phase of cooling was driven by processes occurring in the north. Although the recent rapid regional warming is clearly visible, the Maxwell Bay record does not show the dominance of summer-type sediments until the 1970s. Continued warming in this area will likely affect the marine ecosystem through meltwater induced turbidity of the surface waters as well as an extension of the vegetation period due to the predicted decrease of sea ice in this area.

Costarelli Brandi, Hugo, Pulchrum: Origen y originalidad del quae visa placent en Santo Tomás de Aquino. Cuadernos de Anuario Filosófico 228, Servicio de publicaciones de la Universidad de Navarra, Pamplona, 2010, ISSN 1137-2176, 153 pp.

Fil: Juri, María Agustina.